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First International Electronic Conference on the Hydrological Cycle
12–16 Nov 2017
- Go to the Sessions
-
- A. Global Distribution of Water Vapor
- B. Source-Sink Relationships and Methodologies
- C. Global Source and Sink Regions of Moisture and Processes
- D. Extreme Events
- E. Low-Level Jets, Warm Pools, Monsoons
- F. Paleoclimatic Studies
- G. Climate Change impact on Hydrology
- H. Soil Hydrological Processes
- I. Eco-Hydrology
- J. Water Resources Management
- Event Details
Welcome from the Chairs
Welcome from the Conference Chair
It is a great pleasure to welcome you to the 1st International Electronic Conference on the Hydrological Cycle (CHyCle-1), whose main aim is to advance towards a better understanding of the hydrological cycle, including its observed changes and projections under future climate.
As the first conference in an annual series, the range of topics will be very general, but covering mainly the following subtopics:
i) Global Distribution of Water Vapor: evaporation and precipitation, water vapor flux and divergence, long-range transport of water vapor,
ii) Source-Sink Relationships: methods used to establish source-receptor relationships, analytical or box models, numerical water vapor tracers, physical water vapor tracers (isotopes),
iii) Global Source and Sink Regions of Moisture: oceanic sources, terrestrial sources,
iv) Extreme Events: Atmospheric Rivers, floods, evaporation Hot Spots, anomalies of moisture transport linked to Drought Periods,
v) Low-Level Jets, Warm Pools, Monsoons and their role in the transport of moisture,
vi) the identification and characteristics of moisture sources, megadroughts, and megapluvials within the scope of Palaeoclimatic studies,
vii) implications of Climate Change for Hydrology: changes in water vapor, changes in large-scale circulation related to moisture transport, changes in precipitation, aridity, evapotranpiration, soil moisture, streamflow and other usable water sources (snow, lake levels, reservoirs, glaciers, etc.).
viii) impacts of climate change in Soil Hydrological Processes, with special focus on forest hydrology, including experimental plots and catchments.
ix) Eco-hydrological modelling at different spatial scales.
x) Water resources management and impacts of climate change, including adaptation strategies, with special focus in the Mediterranean region.
This is a virtual conference sponsored by the open access journal Water (https://www.mdpi.com/journal/water)
The participation is free of charge—both for authors and attendees. Selected papers will be published in the journal Water, through invitation from the CHyCle-1 conference chair.
Water (ISSN 2073-4441; CODEN: WATEGH) is an open access journal on water science and technology, including the ecology and management of water resources, and is published monthly online by MDPI.
Open Access: free for readers, with publishing fees paid by authors or their institutions.
High visibility: indexed by the Science Citation Index Expanded (Web of Science), Scopus (Elsevier) and other databases.
Rapid publication: manuscripts are peer-reviewed and a first decision provided to authors approximately 29 days after submission; acceptance to publication is undertaken in 7 days (median values for papers published in this journal in 2016).
Impact Factor: 1.687 (2015); 5-Year Impact Factor: 1.912 (2015)
Call for Papers
Call for Papers closed
The 1st International Electronic Conference on Hydrological Cycle (CHyCle-2017) will be held from 12-16 November 2017 online. This event enables the researchers to present their results and exchange ideas with their colleagues without the need to travel. All proceedings will be published on the conference homepage in open access format.
Through this event, we aim to cover the following topics:
- Global Distribution of Water Vapor (Section A)
- Source-Sink Relationships and Methodologies (Section B)
- Global Source and Sink Regions of Moisture of Moisture and Processes (Section C)
- Extreme Events (Section D)
- Low-Level Jets, Warm Pools, Monsoons (Section E)
- Paleoclimatic studies (Section F)
- Climate Change for Hydrology (Section G)
- Soil Hydrological Processes (Section H)
- Eco-hydrological modelling (Section I)
- Water resources management and impacts of climate change (Section J)
The conference will be completely free of charge—both to attend and for scholars to upload and present their latest work on the conference platform. We would like to invite you to “attend” this conference and present your latest works.
CHyCle-2017 is sponsored by MDPI, a scholarly open access publisher based in Basel, Switzerland.
There will also be the possibility to submit your(s) paper(s) to the journal Water (ISSN 2073-4441; Impact Factor: 1.687; 5-Year Impact Factor: 1.912) in a Special Issue with a 10% discount on the Article Processing Charges (APCs).
There will be three Best Proceeding Paper Award: The 3 best proceeding papers selected by the Scientific Committee after the conference will be published as a full paper for free in the Waters Special Issue after peer-review, in case of being accepted.
The winners will be announced on 5 December 2017.
Abstracts (in English) should be submitted by 25 September 2017 online at https://www.sciforum.net/login. For accepted abstracts, the full paper can be submitted by 5 December 2017. The conference itself will be held 12-16 November 2017.
Paper Submission Guidelines
For information about the submission procedure and preparation of a full presentation, please refer to the "Instructions for Authors".
We hope you will be able to join this exciting event and support us in making it a success.
Conference Chairs
Sessions
A. Global Distribution of Water VaporB. Source-Sink Relationships and Methodologies
C. Global Source and Sink Regions of Moisture and Processes
D. Extreme Events
E. Low-Level Jets, Warm Pools, Monsoons
F. Paleoclimatic Studies
G. Climate Change impact on Hydrology
H. Soil Hydrological Processes
I. Eco-Hydrology
J. Water Resources Management
Instructions for Authors
Submissions should be done by the authors online by registering with www.sciforum.net, and using the "Start New Submission" function once logged into system.
- Scholars interested in participating with the conference can submit their abstract (about 150-300 words covering the areas of manuscripts for the proceedings issue) online on this website until 25 September 2017.
- The Conference Committee will pre-evaluate, based on the submitted abstract, whether a contribution from the authors of the abstract will be welcome for the CHyCle-2017. All authors will be notified by 1 October 2017 about the acceptance of their abstract.
- If the abstract is accepted for this conference, the author is asked to submit his/her manuscript until the submission deadline of 5 November 2017.
- The manuscripts and presentations will be available on CHyCle-2017 homepage for discussion and rating during the time of the conference 12-16 November 2017.
- Accepted papers will be published in the proceedings of the conference. After the conference, the authors are recommended to submit an extended version of the proceeding papers to the Water Special issue with 10% discount on the APC.
Manuscripts for the proceedings issue must have the following organization:
- Title
- Full author names
- Affiliations (including full postal address) and authors' e-mail addresses
- Abstract
- Keywords
- Introduction
- Methods
- Results and Discussion
- Conclusions
- (Acknowledgements)
- References
Manuscripts should be prepared in MS Word and should be converted to the PDF format before submission. The publication format will be PDF. There is no page limit on the length, although authors are asked to keep their papers as concise as possible.
Accepted File FormatsMicrosoft Word
Authors must use the Microsoft Word template to prepare their manuscript. Using the template file will substantially shorten the time to complete copy-editing and publication of accepted manuscripts. Manuscript prepared in MS Word must be converted into a single file before submission. Please do not insert any graphics (schemes, figures, etc.) into a movable frame which can superimpose the text and make the layout very difficult.
- Paper Format: A4 paper format, the printing area is 17.5 cm x 26.2 cm. The margins should be 1.75 cm on each side of the paper (top, bottom, left, and right sides).
- Formatting / Style: Papers should be prepared following the style of CHyCle-2017 template. The full titles and the cited papers must be given. Reference numbers should be placed in square brackets [ ], and placed before the punctuation; for example [4] or [1-3], and all the references should be listed separately and as the last section at the end of the manuscript.
- Authors List and Affiliation Format: Authors' full first and last names must be given. Abbreviated middle name can be added. For papers written by various contributors a corresponding author must be designated. The PubMed/MEDLINE format is used for affiliations: complete street address information including city, zip code, state/province, country, and email address should be added. All authors who contributed significantly to the manuscript (including writing a section) should be listed on the first page of the manuscript, below the title of the article. Other parties, who provided only minor contributions, should be listed under Acknowledgments only. A minor contribution might be a discussion with the author, reading through the draft of the manuscript, or performing English corrections.
- Figures, Schemes and Tables: Authors are encouraged to prepare figures and schemes in color. Full color graphics will be published free of charge. Figure and schemes must be numbered (Figure 1, Scheme I, Figure 2, Scheme II, etc.) and a explanatory title must be added. Tables should be inserted into the main text, and numbers and titles for all tables supplied. All table columns should have an explanatory heading. Please supply legends for all figures, schemes and tables. The legends should be prepared as a separate paragraph of the main text and placed in the main text before a table, a figure or a scheme.
For further enquiries please contact the Conference Secretariat.
It is the authors' responsibility to identify and declare any personal circumstances or interests that may be perceived as inappropriately influencing the representation or interpretation of clinical research. If there is no conflict, please state here "The authors declare no conflict of interest." This should be conveyed in a separate "Conflict of Interest" statement preceding the "Acknowledgments" and "References" sections at the end of the manuscript. Financial support for the study must be fully disclosed under "Acknowledgments" section. It is the authors' responsibility to identify and declare any personal circumstances or interests that may be perceived as inappropriately influencing the representation or interpretation of clinical research. If there is no conflict, please state here "The authors declare no conflict of interest." This should be conveyed in a separate "Conflict of Interest" statement preceding the "Acknowledgments" and "References" sections at the end of the manuscript. Financial support for the study must be fully disclosed under "Acknowledgments" section.
CopyrightMDPI AG, the publisher of the Sciforum.net platform, is an open access publisher. We believe that authors should retain the copyright to their scholarly works. Hence, by submitting a Communication paper to this conference, you retain the copyright of your paper, but you grant MDPI AG the non-exclusive right to publish this paper online on the Sciforum.net platform. This means you can easily submit your paper to any scientific journal at a later stage and transfer the copyright to its publisher (if required by that publisher).
List of accepted submissions (39)
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sciforum-014156 | Drought and wet episodes in Amazonia: the role of atmospheric moisture transport | , , , , | N/A |
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The Amazon River basin (ARB) in Sud-America contains the world largest rainforest and biodiversity and plays an important role in the regional and global hydrological cycle. It consist of several sub-basins as the Negro River basin (NRB) in the north and the Madeira River basin (MRB) to the south, both considered of utmost importance in the Amazonia for the Amazon River. The precipitation annual cycle in both basins experiences an opposite annual cycle and as a consequence their contributions to the Amazon River are lagged in time. Here we utilized the Standardized Precipitation Index (SPEI) to identify drought and wet conditions in the NRB and MRB along the period 1980-2016. This index has the advantages over other index because considers the effect of the Atmospheric Evaporation Demand (AED) on drought severity. Besides, the Lagrangian dispersion model FLEXPART v9.0 was used to track backward in time air masses residing over the basins and to calculate along the trajectories the budget of (E-P). This permitted to identify those regions from where air masses gain humidity (E-P>0) before arriving at the basins, what we consider as moisture sources. FLEXPART has been successfully utilized for the same goal in several studies. This allowed investigating the hydrological budget of (E-P) over the NRB and MRB as well as their role as sources of moisture for surrounded continental regions. This study examines the variability of moisture uptake by the basins from these sources during drought and wet episodes in the basins. We consider this a new approach to be a useful method for understanding the causes and variability of drought and wet events in other regions worldwide. |
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sciforum-014133 | Tagging moisture sources with Eulerian and Lagrangian tracers: Application to an intense atmospheric river event. | , , , | N/A |
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One Eulerian and two Lagrangian tracers’ tools are evaluated for studies on atmospheric moisture sources and pathways. The first method has been recently implemented online into the Weather Research and Forecasting (WRF) mesoscale model (Insua-Costa and Míguez-Macho, 2017), while the Lagrangian methods are described here. In these methods, a moisture volume is assigned to each particle which is then advected by the wind flow. Usual Lagrangian methods consider this volume to remain constant and the particle follows exactly the stream lines of the flow (Stohl and James, 2004). On the other hand, the initial moisture volume can be thought to depend on time as the flow is advected due to thermodynamic processes (for example, pressure, and temperature changes). In this case, the drag on the tracer volume must be taken into account. Equations have been implemented and moisture convection (Forster et al., 2007) was taken into account for both Lagrangian models. We apply these methods to evaluate the intense atmospheric river (AR; i.e., a narrow plume of strong water vapor flux) that devastated the Pacific North Western America with flooding rains and intense winds in early November 2006 (Neiman et al., 2008). We note that the usual Lagrangian method underestimate moisture availability on the continent while the active tracers (both Eulerian and Lagrangian) achieve better results.
Forster, C., Stohl, A. and Seibert, P. J. Applied Meteo. and Climatology. 46, 403 (2007). Insua-Costa, D. and Míguez-Macho, G. Eath Syst. Dyn. (2017). Neiman, P.J. et al. Monthly Wea. Rev. 136, 4398 (2008). Stohl, A. and James, P. J. Hidrometeor. 5, 656 (2004). |
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sciforum-013942 | ANALYSIS OF THE VARIABILITY OF WATER LEVELS OF TITICACA LAKE | , |
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The purpose of this research was to compare the variability of the Titicaca Lake water level to the Pacific Decadal Oscillation (PDO) between 1914 and 2014 and relate it was compared to El Niño - Southern Oscillation (ENSO) between 1969 and 2014 to evalute the hydrological cycle and perform rainfall forecast. The results show that the Lake Titicaca water level to decrease (increase) in the positive (negative) phase of the PDO. Likewise, the negative phase (positive) of ENSO generates patterns of positive anomalies (negative) of precipitation. Therefore, the positive (negative) phase of PDO, with greater probability of positive phase ENSO events (negative), precipitation anomalies shows negative (positive) which can be associated with the decrease (increase) in Titicaca Lake water level. |
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sciforum-014059 | The influence of climate and land-cover scenarios on dam management strategies in a high water pressure catchment in North-east Spain | , , , , , , , , | N/A |
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The water management of Boadella-Darnius reservoir (NE Spain) has been analysed for the period 1971-2013 to understand the different strategies applied in the past. Streamflow has been projected under climate conditions included in the Third Report on Climate Change in Catalonia (TCCC) and under land-use change scenarios. We have simulated Darnius-Boadella reservoir inflow (2021-2050) using the Regional Hydro-Ecologic Simulation System (RHESsys) with two objectives: (i) to analyse the impact of climate and land-use changes on the water resources of the basin and (ii) to analyse the different plausible strategies of water management at mid-term period (2021-2050). Results reveal a clear negative trend in dam inflow (-34.7%) since it was built in 1971. The simulations obtained with RHESsys show a similar trend at mid-term (2021-2050) with -31.1% under climate and land-use change conditions. Considering the ecological minimum flow outlined by Catalan Water Agency (ACA) and the possible dam inflow decrease, different water management strategies are needed to mitigate the effects of the expected climate change. |
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sciforum-014017 | Patterns of atmospheric moisture transport linked to Southern Ocean Sea ice coverage changes | , , , , , | N/A |
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Moisture sources identification and Sea Ice Concentration (SIC) were calculated for the period 1980-2016 for the Southern Ocean Sea. Five sectors of the Southern Ocean Sea (King Hakon VII, East Antarctic, Ross/Amundsen, Amundsen and Bellingshausen, Weddell) were selected to calculate their moisture sources. The results show that the most important moisture sources (calculated as positive values of Evaporation minus Precipitation, E-P>0) for these five seas come from extratropical latitudes in the storm track trajectories. The main moisture sources and affected regional seas are: Southern Australia (SAUS) moisture source which affect mainly Ross/Amundsen and Amundsen and Bellingshausen seas; the Atlantic Ocean is the main source of moisture for Weddell and King Hakon VII; and the Pacific Ocean provides moisture to Ross/Amundsen, Weddell and Amundsen and Bellingshausen seas. For most of these seas it was identified positive trends of E-P>0 anomalies, while negative trends were identified only for the SAUS moisture source to Amundsen and Bellingshausen Sea. In terms of SIC, for the whole Antarctic the total anomalies are increasing, but no breaking points in this time serie were detected. Preliminary results also indicate some areas, which do not coincide exactly with the limit of the regional seas, where the increase of Sea Ice Extension (SIE) is statistically significant. |
List of Authors (113)
About This Conference
The main aim of this International Electronic conference is to advance towards a better understanding of the Hydrological Cycle, including its observed changes and projections under future climate.
As the first conference in an annual series, the range of topics will be very general, but covering mainly the following subtopics:
i) Global Distribution of Water Vapor: evaporation and precipitation, water vapor flux and divergence, long-range transport of water vapor, clouds,
ii) Source-Sink Relationships and Methodologies: methods used to establish source-receptor relationships, analytical or box models, numerical water vapor tracers, physical water vapor tracers (isotopes),
iii) Global Source and Sink Regions of Moisture and Processes: identifying large-scale oceanic sources, terrestrial sources, and sinks of moisture, investigating the mechanisms associated with source and sink regions,
iv) Extreme Events: Atmospheric Rivers, floods, evaporation Hot Spots, anomalies of moisture transport linked to Drought Periods,
v) Low-Level Jets, Warm Pools, Monsoons and their role in the transport of moisture,
vi) the identification and characteristics of moisture sources, megadroughts, and megapluvials within the scope of Paleoclimatic studies,
vii) implications of Climate Change for Hydrology: changes in water vapor, changes in large-scale circulation related to moisture transport, changes in precipitation, aridity, evapotranpiration, soil moisture, streamflow, cloud distribution, and other usable water sources (snow, lake levels, reservoirs, glaciers, etc.).
viii) impacts of climate change in Soil Hydrological Processes, with special focus on forest hydrology, including experimental plots and catchments.
ix) Eco-hydrological modelling at different spatial scales.
x) Water resources management and impacts of climate change, including adaptation strategies, with special focus in the Mediterranean region.
Conference Schedule
Abstract Submission: 25 Sep. 2017 (closed)
Acceptance Notification: 1 Oct. 2017 (closed)
Full Proceeding Submission: 8 Nov. 2017 (closed)
Best Proceeding Paper Award: 5 Dec. 2017 (see "Proceedings & Editors")
FULL PAPER Submission to WATER Special Issue: 30 SEPTEMBER 2018
Conference Organizers
Conference Chair
Dr. Raquel Nieto, Environmental Physics Laboratory (EPhysLab), Facultade de Ciencias, Universidade de Vigo, Ourense, Spain.
E-mail: [email protected]
Conference Co-Chair
Dr. Luis Gimeno, Environmental Physics Laboratory (EPhysLab), Facultade de Ciencias, Universidade de Vigo, Ourense, Spain.
E-mail: [email protected]
Proceedings & Editors
The Conference Committee has decided that the BEST PROCEEDING AWARDS go to:
1º: The role of ocean variability for droughts and wet periods in South America by A. Taschetto
2º: A lagrangian analysis of the moisture transport during the 2003 drought episode over the Mediterranean region by M. Stojanovic et al.
3º: Extreme drought events over Amazon basin: the perspective from regional reconstruction of South American hydroclimate by B. Garcia et al.
4º: Drought and wet episodes in Amazonia: the role of atmospheric moisture transport by R. Sorí at al.
These best proceedings will be published as a FULL PAPER for FREE in the WATER Special Issue after peer-review, in case of being accepted.
Dead-line for submission: 30 September 2018
CD-ROM edition
There is currently no CD-ROM available
A. Global Distribution of Water Vapor
Global Distribution of Water Vapor: evaporation and precipitation, water vapor flux and divergence, long-range transport of water vapor, clouds.
This section is chaired by:
Dr. Ana María Durán-Quesada, Centre for Geophysical Research, University of Costa Rica, San José, Costa Rica.
Dr. Anita Drumond, Environmental Physics Laboratory (EPhysLab), Facultade de Ciencias, Universidade de Vigo, Ourense, Spain.
Dr. Rosana Nieto-Ferreira, Department of Geography, Planning and Environment, East Carolina University, Greenville, North Carolina, USA.
B. Source-Sink Relationships and Methodologies
Source-Sink Relationships and Methodologies: methods used to establish source-receptor relationships, analytical or box models, numerical water vapor tracers, physical water vapor tracers (isotopes).
This section is chaired by:
Dr. Ana María Durán-Quesada, Centre for Geophysical Research, University of Costa Rica, San José, Costa Rica.
Dr. Anita Drumond, Environmental Physics Laboratory (EPhysLab), Facultade de Ciencias, Universidade de Vigo, Ourense, Spain.
C. Global Source and Sink Regions of Moisture and Processes
Global Source and Sink Regions of Moisture and Processes: identifying large-scale oceanic sources, terrestrial sources, and sinks of moisture, investigating the mechanisms associated with source and sink regions.
This section is chaired by:
Dr. Ana María Durán-Quesada, Centre for Geophysical Research, University of Costa Rica, San José, Costa Rica.
Dr. Anita Drumond, Environmental Physics Laboratory (EPhysLab), Facultade de Ciencias, Universidade de Vigo, Ourense, Spain.
Dr. Francina Dominguez, Department of Atmospheric Sciences, University of Illinois, Urbana, Illinois, USA.
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D. Extreme Events
Atmospheric Rivers, Floods, Evaporation Hot Spots, anomalies of moisture transport linked to Drought Periods
This section is chaired by:
Dr. Ana María Durán-Quesada, Centre for Geophysical Research, University of Costa Rica, San José, Costa Rica.
Dr. Andréa S. Taschetto, Climate Change Research Centre & Australian Research Council Centre of Excellence for Climate System Science, University of New South Wales, Sydney, Australia.
Dr. Anita Drumond, Environmental Physics Laboratory (EPhysLab), Facultade de Ciencias, Universidade de Vigo, Ourense, Spain.
Dr. José A. Marengo, National Center for Monitoring and Early Warning of Natural Disasters (CEMADEN), Sao José dos Campos, Brazil.
Dr. Moncho G. Gesteira, Environmental Physics Laboratory (EPhysLab), Facultade de Ciencias, Universidade de Vigo, Ourense, Spain
Dr. Ricardo M. Trigo, Instituto Dom Luiz (IDL), Faculdade de Ciências, Universidade de Lisboa, Lisbon, Portugal.
Dr. Rosana Nieto-Ferreira, Department of Geography, Planning and Environment, East Carolina University, Greenville, North Carolina, USA.
Dr. Sergio M. Vicente-Serrano, Pyrenean Institute of Ecology, IPE-CSIC, Zaragoza, Spain.
Dr. Tercio Ambrizzi, Institute of Astronomy, Geophysics and Atmospheric Sciences (IAG), São Paulo, SP, Brazil.
E. Low-Level Jets, Warm Pools, Monsoons
Low-Level Jets, Warm Pools, Monsoons and their role in the transport of moisture.
This section is chaired by:
Dr. Ana María Durán-Quesada, Centre for Geophysical Research, University of Costa Rica, San José, Costa Rica.
Dr. Anita Drumond, Environmental Physics Laboratory (EPhysLab), Facultade de Ciencias, Universidade de Vigo, Ourense, Spain.
Dr. Andréa S. Taschetto, Climate Change Research Centre & Australian Research Council Centre of Excellence for Climate System Science, University of New South Wales, Sydney, Australia.
Dr. José A. Marengo, National Center for Monitoring and Early Warning of Natural Disasters (CEMADEN), Sao José dos Campos, Brazil.
Dr. Rosana Nieto-Ferreira, Department of Geography, Planning and Environment, East Carolina University, Greenville, North Carolina, USA.
Dr. Victor Magaña, Geography Institute, Universidad Autónoma de México (UNAM), México.
F. Paleoclimatic Studies
The identification and characteristics of moisture sources, megadroughts, and megapluvials within the scope of Palaeoclimatic studies.
This section is chaired by:
Dr. Ricardo M. Trigo, Instituto Dom Luiz (IDL), Faculdade de Ciências, Universidade de Lisboa, Lisbon, Portugal.
Dr. Tercio Ambrizzi, Institute of Astronomy, Geophysics and Atmospheric Sciences (IAG), São Paulo, SP, Brazil.
G. Climate Change impact on Hydrology
Implications of Climate Change impact on Hydrology: response of the terrestrial and atmospheric branches of the hydrological cycle to long-term changes in atmospheric composition and land use, including impacts on large-scale evaporation, soil moisture, precipitation, water vapour, aridity, streamflow, cloud distribution, and other water resources (like e.g., snow depths, lake levels, reservoirs, glaciers).
This section is chaired by:
Dr. Adriana Cuartas, National Center for Monitoring and Early Warning of Natural Disasters (CEMADEN), Sao José dos Campos, Brazil.
Dr. Diego Miralles, Laboratory of Hydrology and Water Management, Ghent University, Ghent, Belgium.
Dr. José A. Marengo, National Center for Monitoring and Early Warning of Natural Disasters (CEMADEN), Sao José dos Campos, Brazil.
Dr. Sergio M. Vicente-Serrano, Pyrenean Institute of Ecology, IPE-CSIC, Zaragoza, Spain.
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H. Soil Hydrological Processes
Impacts of climate change in Soil Hydrological Processes, with special focus on forest hydrology, including experimental plots and catchments.
This section is chaired by:
Dr. Sergio M. Vicente-Serrano, Pyrenean Institute of Ecology, IPE-CSIC, Zaragoza, Spain.
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I. Eco-Hydrology
Eco-Hydrology: studies of the two-way coupling between hydrology and vegetation, both from a modelling perspective (e.g. conceptual, hydrological and climate models) and observational perspective (field experiments, remote sensing), including the full spectrum of spatio-temporal scales.
This section is chaired by:
Dr. Diego Miralles, Laboratory of Hydrology and Water Management, Ghent University, Ghent, Belgium.
Dr. Sergio M. Vicente-Serrano, Pyrenean Institute of Ecology, IPE-CSIC, Zaragoza, Spain.
Dr. Adriana Cuartas, National Center for Monitoring and Early Warning of Natural Disasters (CEMADEN), Sao José dos Campos, Brazil
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J. Water Resources Management
Water resources management and impacts of climate change, including adaptation strategies, with special focus in the Mediterranean region.
This section is chaired by:
Dr. Sergio M. Vicente-Serrano, Pyrenean Institute of Ecology, IPE-CSIC, Zaragoza, Spain.
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